Storm Ready

California's historic drought remains severe, and residents must continue to conserve water. At the same time, we must also prepare for the possibility of large storms and coastal/bay flooding.

Storms in California sometimes cause flooding, mud flows, landslides, electrical outages and other impacts.

Using water wisely while taking steps to prepare for winter storms and coastal/bay flooding will help to protect our households, our communities and our state.

Information on this website updates weather conditions and shares what Californians can also do to prepare.

An overview of preparedness for winter storms can be found on the State's Winter Readiness Fact Sheet.

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The types of storms that have been bringing heavy snow and rain to the West this winter, triggering landslides and floods while easing stubborn droughts, are likely to become stronger and more frequent, according to the results of a conclusive new study. Read More>

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California broke a record late last month: Sea levels at several tide stations in Southern California reached higher elevations than ever measured before, including during major storms. Water levels were higher than the “King Tides” that were predicted by the National Oceanic and Atmospheric Administration (NOAA), due to the ongoing El Niño, warm ocean temperatures and a minor storm. NOAA observations for San Diego, La Jolla and Santa Barbara show sea levels for November 25, 2015 higher than the maximum water levels ever recorded at these tide stations. Read More>

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The stage is set for a strong El Niño event this winter, but experts are cautioning that heavy rain and even flooding in some parts of the state will not necessarily end California's four-year drought. While there is no single factor that will determine when the drought ends, water managers and other experts will be watching several factors for signs of improvement. ACWA has prepared an infographic (.pdf) with a high-level look at key drought recovery factors and several unknowns that may come into play. Read More>

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